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P-class asteroids are a taxonomic classification of asteroids characterized by their low albedo (reflectivity) and a featureless spectral reflectance that slopes upward into the red. They have a mean albedo of 0.04.1

Currently, there are no known meteorite or naturally occurring mineralogical counterparts for P-class asteroids. However, it is theorized that their surface material may contain a significant fraction of carbon polymers or organic-rich silicates, or both.1

While P-class asteroids are not the most common type in the asteroid belt, they constitute about 4 percent of the larger asteroids (those with diameters greater than 25 km). They are found in the outer regions of the asteroid belt, dominating populations at distances of about 5 AU from the Sun.12

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